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This article in JEQ

  1. Vol. 27 No. 5, p. 1125-1129
     
    Received: Oct 27, 1997
    Published: Sept, 1998


    * Corresponding author(s): wwood@acesag.auburn.edu
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doi:10.2134/jeq1998.00472425002700050018x

Ammonia Volatilization from Tall Fescue Pastures Fertilized with Broiler Litter

  1. S. B. Marshall,
  2. C. W. Wood *,
  3. L. C. Braun,
  4. M. L. Cabrera,
  5. M. D. Mullen and
  6. E. A. Guertal
  1. Dep. of Agronomy and Soils, 202 Funchess Hall, Auburn Univ., AL 36849-5412;
    Dep. of Crop and Soil Sciences, Univ. of Georgia, Athens, GA 30602-7272;
    Dep. of Plant and Soil Sciences, Univ. of Tennessee, Knoxville, TN 37901-1071.

Abstract

Abstract

Ammonia (NH3) volatilization is an important and often overlooked component of the N budget in many agricultural systems involving land application of animal wastes. We quantified the amount and rate of NH3 volatilization from broiler litter applied to established tall fescue pastures (Festuca arundinacea Schreb.). Study sites were located in the Coastal Plain (Alabama), Piedmont (Georgia), and Cumberland Plateau (Tennessee) Major Land Resource Areas (MLRA) of the southeast USA. Litter was applied to supply 70 kg of available N ha−1 based on equations developed by the U.S. Department of Agriculture (USDA) and the U.S. Environmental Protection Agency (USEPA). Measurements of NH3-N volatilization were taken using a micrometeorological, field-scale technique for 14 d immediately following litter application during the spring of 1995 and 1996. Ammonia flux for the study period ranged from 3.7 to 10.6 kg N ha−1 in 1995, and from 3.5 to 8.0 kg N ha−1 in 1996. A sharp increase in volatilization rate occurred 1 to 3 d after litter application at all three sites in both years. However, volatilization rates rapidly decreased to normal levels within 10 d. Volatilization rates peaked at 2.8 kg NH3-N ha−1 d−1 in 1995 and 2.2 kg NH3-N ha−1 d−1 in 1996. Overall, N losses due to NH3 volatilization were less than expected based on previous studies. These data suggest that for these conditions, NH3 volatilization was a relatively minor component of the N cycle and was not a major pathway for N loss.

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